500 years of regional forest growth variability and links to climatic extreme events in Europe

被引:59
作者
Babst, Flurin [1 ]
Carrer, Marco [2 ]
Poulter, Benjamin [3 ]
Urbinati, Carlo [4 ]
Neuwirth, Burkhard [5 ]
Frank, David [1 ,6 ]
机构
[1] Swiss Fed Res Inst WSL, CH-8903 Birmensdorf, Switzerland
[2] Univ Padua, TeSAF Dept, Forest Ecol Res Unit, Legnaro, PD, Italy
[3] Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
[4] Univ Politecn Marche, I-60121 Ancona, Italy
[5] DeLaWi Tree Ring Anal, D-51570 Windeck, Germany
[6] Oeschger Ctr Climate Change, CH-3012 Bern, Switzerland
来源
ENVIRONMENTAL RESEARCH LETTERS | 2012年 / 7卷 / 04期
基金
瑞士国家科学基金会;
关键词
network; productivity; high frequency; extreme event; reconstruction; tree-ring; lag effect; autocorrelation; CARBON-CYCLE; NORTHERN-HEMISPHERE; TREE-GROWTH; ABIES-ALBA; TEMPERATURE; SENSITIVITY; RECONSTRUCTION; VULNERABILITY; CAPACITY; DENSITY;
D O I
10.1088/1748-9326/7/4/045705
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climatic extreme events strongly affect forest growth and thus significantly influence the inter-annual terrestrial carbon balance. As we are facing an increase in frequency and intensity of climate extremes, extensive empirical archives are required to assess continental scale impacts of temperature and precipitation anomalies. Here we divide a tree-ring network of approximately 1000 sites into fifteen groups of similar high-frequency growth variability to reconstruct regional positive and negative extreme events in different parts of Europe between 1500 and 2008. Synchronized growth maxima or minima within and among regions indicate eighteen years in the pre-instrumental period and two events in the 20th century (1948, 1976) with extensive radial growth fluctuations. Comparisons with instrumental data showed that the European tree-ring network mirrors the spatial extent of temperature and precipitation extremes, but the interpretation of pre-instrumental events is challenged by lagged responses to off-growing season climate extremes. We were able to attribute growth minima in subsequent years to unfavourable August-October conditions and to mild climate during winter months associated with respiratory carbon losses. Our results emphasize the importance of carry-over effects and species-specific growth characteristics for forest productivity. Furthermore, they promote the use of regional tree-ring chronologies in research related to climate variability and terrestrial carbon sink dynamics.
引用
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页数:11
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